Continental signature of a ridge‐trench‐triple junction: Northern Vancouver Island
- 10 April 1997
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 102 (B4) , 7767-7781
- https://doi.org/10.1029/96jb03899
Abstract
No abstract availableKeywords
This publication has 51 references indexed in Scilit:
- Basalt geochemistry used to investigate past tectonic environments on CyprusPublished by Elsevier ,2003
- Crustal structure of the Cascadia subduction zone, southwestern British Columbia, from potential field and seismic studiesCanadian Journal of Earth Sciences, 1997
- Crustal thickness beneath the Queen Charlotte Basin, Canada: Results of a seismically constrained gravity inversionJournal of Geophysical Research, 1995
- Ephemeral plate tectonics at the Queen Charlotte triple junctionGeology, 1995
- Geology, geochemistry and petrogenesis of Middle Tertiary volcanic rocks of the Queen Charlotte Islands, British Columbia (Canada)Journal of Volcanology and Geothermal Research, 1993
- Influence of terrain on bedrock temperaturesGlobal and Planetary Change, 1992
- Integrated geophysical modelling of terranes and other structural features along the western Canadian marginCanadian Journal of Earth Sciences, 1992
- The Neogene Alert Bay Volcanic Belt of northern Vancouver Island, Canada: Descending-plate-edge volcanism in the arc-trench gapJournal of Volcanology and Geothermal Research, 1985
- Heat flux measurements in southwestern British Columbia: the thermal consequences of plate tectonicsCanadian Journal of Earth Sciences, 1985
- Gravity and structure of an active margin—British Columbia and WashingtonCanadian Journal of Earth Sciences, 1979